HR: 17:50h
AN: MR44A-07 [Abstracts]
TI: Phase stability and shear softening in CaSiO3 perovskite at high pressure
AU: * Stixrude, L
EM: stixrude@umich.edu
AF: University of Michigan, Department of Geological Sciences, University of Michigan, Ann
Arbor, MI 48109-1005, United States
AU: Lithgow-Bertelloni, C
EM: crlb@umich.edu
AF: University of Michigan, Department of Geological Sciences, University of Michigan, Ann
Arbor, MI 48109-1005, United States
AU: Kiefer, B
EM: bkiefer@physics.nmsu.edu
AF: New Mexico State University, Department of Physics, New Mexico State University, Las
Cruces, NM 88003, United States
AU: Fumagalli, P
EM: patrizia.fumagalli@unimi.it
AF: Università degli Studi di Milano, Dipartimento di Scienze della Terra, Università degli Studi
di Milano, Milano, Italy
AB:
We predict the phase diagram of CaSiO3 perovskite, finding the tetragonal I4/mcm structure transforming
to cubic Pm3̆m with increasing temperature. The transition temperature is 1150 K at 0 GPa, and 2450 K
at 140 GPa. The c/a ratio of the tetragonal structure is 1.018 at 100 GPa and increases on compression, as
does the static enthalpy difference between tetragonal and cubic structures. The elastic constants of the
tetragonal phase at static conditions differ substantially from those of the cubic phase with the Voigt-Reuss-Hill
shear modulus 29 % less at 100 GPa. Computations are based on density functional theory in the local density
and generalized gradient approximations. The phase diagram and high temperature elastic constants are
computed using a mean field theory with parameters of the Landau potential determined via structurally
constrained density functional theory calculations. We present a simple scheme for systematically searching for
the ground state over all perovskite structures derivable from octahedral rotations within the context of symmetry-
preserving relaxation, which confirms tetragonal I4/mcm as the ground state in density functional theory. We
argue that the experimental x-ray diffraction pattern can be explained by the I4/mcm phase by considering the
development of preferred orientation under uniaxial compression.
DE: 3909 Elasticity and anelasticity
DE: 3924 High-pressure behavior
SC: Mineral and Rock Physics [MR]
MN: 2007 Joint Assembly